MET 2204 METEOROLOGY

MET 2204METEOROLOGY Presentation 7: Turbulence Presented by Mohd Amirul for AMC

Recapitulate Lets recap what we have done last week: • Definition of Thunderstorm. • Time and location of Thunderstorm can occur. • Three stages of Thunderstorm’s formation. • Size of Thunderstorm. • Types of Thunderstorm. • Hazards of Thunderstorm. • Do’s and Don’ts flying in Thunderstorm. • Weather Radar. Presented by Mohd Amirul for AMC

Presentation Outline • Introduction • Convective Turbulence • Obstruction to wind flow • Wind Shear • Wake Turbulence • Conclusion Presented by Mohd Amirul for AMC

Learning Outcomes • At the end of this session, student should be able to: • Understand the concept of turbulence, their caused and some rule in flying turbulence Presented by Mohd Amirul for AMC

Introduction • Turbulence: Irregular motion of the atmosphere where air currents vary greatly over the short distances. • This air currents range from mild eddies to strong currents of relatively large dimensions. • If aircraft moves through this currents, it will undergoes changing acceleration which jostle (divert) it from smooth flight path.

Cont. • We call this jostle as TURBULENCE. • Turbulence range from bumpiness (which can annoy crews and passengers) to severe jolts (which can structurally damage the aircraft or injure its passenger).

Cont. • Aircraft reaction to turbulence varies with the difference in: • Wind speed in adjacent current • Size of aircraft • Wing loading • Aircraft altitude • Airspeed / The speed of aircraft travelling from one current to another. • Rapid undergoes sudden changes in acceleration • Slow the changes in acceleration would be more gradual. • Therefore, the first rule in flying turbulence is to reduce airspeed. (a/c manual has list recommendation of airspeed for penetrating the turbulence)

Cont. • Knowing WHEREto expect turbulence helps a pilot avoid or minimize the hazards. • Main cause of turbulence: • Convective Currents (Thermal Turbulence) • Obstruction to wind flow • Wind Shear • Wake Turbulence (Wake of moving aircraft whenever the airfoils exert lift).

1. Convective Current (Thermal Turbulence) • Common cause of turbulence especially at low altitude. • Localized vertical air movements; both ascending and descending. So for every rising current there is downward current. • Downward current frequently occur over broader areas than upward currents. Therefore, it will have slower vertical speed than rising current.

Cont. • Convective current most active on warm summer afternoons when winds are light. • It increases in strength and to the greater height as surface heating increase. • The strength of convective current can vary considerably within short distance. How?? • Barren surface (sandy, rocky) hotter rather than open water or ground covered by vegetation. Therefore, air at and near surface heats unevenly. Because of this uneven heating, the strength of convective currents can be vary considerably within the short distance.

Cont. • When cold air moves over a warm surface, it becomes unstable in lower levels. Convective currents extend several thousand feet above the surface resulting in rough , choppy turbulence when flying in the cold air. • This condition often occurs in any season in the cold fronts. *Cold front: cooler mass of air replacing a warmer mass air

Cont. • Effect of aircraft at low-level convective turbulence on aircraft approach to land: Cause sudden changes in air speed and may even result in a stall at low altitude. • To prevent this danger increase airspeed slightly over normal approach speed but still below the recommended turbulence penetration speed.

Effect of convective currents on final approach. Predominantly upward currents (top) tend to cause the aircraft to overshoot. Predominantly downward currents (bottom) tend to cause the aircraft to undershoot.

Cont. • Air moves upward cool by expansion (expansion cooling). • A convective current continues upward until it reaches a level where its temperature cools to the same as that surrounding air. (if it cool to saturation it will form CLOUD). • Billowy (great swelling waves) fair weather cumulus clouds, usually seen on sunny afternoons, are signposts in the sky indicating CONVECTIVE TURBULENCE. Billowy cumulus weather

Cont. • The cloud top usually marks the approximate upper limit of the convective current. Air generally is smooth over the cloud. • When convection extends to greater height, it develops larger towering cumulus and cumulonimbus clouds.

Avoiding turbulence by flying above convective clouds

2. Obstruction to wind flow. • Obstruction such as buildings, trees and rough terrain disrupt smooth wind flow into a complex short eddies. • This turbulence we classify as “mechanical turbulence” since it result from mechanical disruption (tools or device) of the ambient wind flow. • The wind carries the turbulent eddies downstream. How far?? • Depends on wind speed and stability of the air. Unstable air allows larger eddies to form. Instability breaks up the eddies quickly, while in stable air they dissipate slowly.

Eddy currents formed by wind blowing over uneven ground or over obstructions

Cont. • Can also cause cloudiness near the top of the mechanically disturbed layer. This type of cloudiness will tell whether it is from mechanical or convective mixing. How? • Convective cloud  produce random pattern (several type of cloud) • Mechanical mixing produce stratocumulus clouds in rows or band. The cloud rows developed may be parallel to or perpendicular to wind. Stratocumulus

Cont. • Common object that can cause gusty condition/ mechanical turbulence • airport structures (e.g. hangar, terminal etc.). Surface gust also can create taxi problem • Terrain features like hills and mountains.

Mechanical turbulence in airport area • The airport area is vulnerable (insecure) to mechanical turbulence which can causes gusty surface winds. • For example, when aircraft is in low level approach or a climb, air speed fluctuates in the gusts (strong current of air) and the aircraft may even stall. Therefore during extremely gusty condition, the aircraft need to maintain a margin of airspeed ABOVE normal approach or climb speed to allow for changes in airspeed. (Increasing airspeed above margin speed for approach and climb).

Turbulent air in the landing area

Mechanical turbulence in the Mountains and Hills area. • Mountains and hills can generate turbulence to attitudes much higher than the mountains themselves. Such turbulence is not hazardous but it may be annoying or uncomfortable. • Climb to higher altitude to reduce the turbulence. • But if flying in rugged (topography very uneven) hills and mountains could RESULT  REAL TURBULENCE PROBLEM.

Cont. • When wind speed across mountains exceed about 40 knots (74.08 km/hr) we can predict there is the turbulence. • Where to what extent the turbulence depends largely on STABILITY of the air.

Unstable air crosses a mountain barrier • If the air crossing the mountains is unstable, the turbulence on the windward side is almost certain. (if sufficient moisture present, convective clouds form. This will make turbulence more intense). • A convective clouds over a mountain or along a ridge are some sign of unstable air and turbulence on the windward side and over the mountain crest. Mountain Ridge

Cont. • As the unstable air crosses the barrier (mountain/hill), it will spills down the leeward slope. Often as a violent downdraft. • Sometimes this downward speed exceeds the max. climb rate for the aircraft. Therefore it will drive the aircraft into the mountain side. Lee side: The side of something that is sheltered from the wind Wind flow in mountain areas. Dangerous downdrafts may be encountered on the lee side.

Stable air crosses a mountain barrier • When stable air crosses a mountain barrier, the turbulent situation is somewhat reversed. Air flowing up the windward side is relatively smooth. Wind flow across the barrier is laminar—that is, it tends to flow in layers. • The barrier (e.g. mountain crest, wave crest) may set up waves in these layers. The waves remain nearly stationary while the wind blows rapidly through them. • The wave pattern, is a “standing” or “mountain” wave, so named because it remains essentially stationary and is associated with the mountain. • The wave pattern may extend 100 miles or more downwind from the barrier.

Cont. • Standing waves can be recognized by the following distinctive clouds: • Lenticular, with ragged (irregular) edges (indicating turbulence) • lens-shaped clouds known as “standing lenticular” clouds • Rotor or roll clouds • Cap clouds- Cloud capped at mountain top. altocumulus (ACSL), cirrocumulus (CCSL)

Cont. • Wave crests extend well above the highest mountains, sometimes into the lower stratosphere. • Under each wave crest is a rotary circulation. The “rotor” forms below the elevation of the mountain peaks.Turbulence can be violent in the overturning rotor. • Updrafts and downdrafts in the waves can also create violent turbulence.

Cont. But remember!! • the clouds are not always present to mark the mountain wave. Sometimes, the air is too dry. Always anticipate possible mountain wave turbulence when strong winds of 40 knots or greater blow across a mountain or ridge and the air is stable.

Mountain Flying • How to fly in the mountain area? • When planning a flight over mountainous terrain, gather as much preflight information as possible on cloud reports, wind direction, wind speed, and stability of air. Satellites often help locate mountain waves.

Cont. • What should you look for both during preflight planning and during your inflight observations? • Wind speed • Wind at mountain top level in excess of 25 knots suggests some turbulence. Wind in excess of 40 knots across a mountain barrier issue caution. • Cloud • Stratified (arrange in sequence) clouds mean stable air. Standing lenticular and/or rotor clouds suggest a mountain wave. So, expect turbulence many miles to the lee of mountains and relative smooth flight on the windward side. • Convective clouds on the windward side of mountains mean unstable air; expect turbulence in close proximity to and on either side of the mountain.

Cont. • Altitude • When approaching mountains from the leeward side during strong winds, begin your climb well away from the mountains—100 miles in a mountain wave and 30 to 50 miles otherwise. • Climb to an altitude 3,000 to 5,000 feet above mountain tops before attempting to cross. If unable to make good on your first attempt and you have higher altitude capabilities, you may back off and make another attempt at higher altitude. Sometimes you may have to choose between turning back or detouring the area.

Cont. • Remember!! • Flying mountain passes and valleys is not a safe procedure during high winds. • The mountains funnel the wind into passes and valleys thus increasing wind speed and intensifying turbulence. If winds at mountain top level are strong, go high, or go around. • Surface wind may be relatively calm in a valley surrounded by mountains when wind aloft is strong. If taking off in the valley, climb above mountain top level before leaving the valley. Maintain lateral clearance from the mountains sufficient to allow recovery if caught in a downdraft.

Wind Shear • Wind shear generates eddies between two wind currents of differing velocities. • The differences may be in wind speed, wind direction, or both. • Three conditions are of special interest— (1) wind shear with a low-level temperature inversion, (2) wind shear in a frontal zone, and (3) clear air turbulence (CAT) at high levels associated with a jet stream or strong circulation.

Wind Shear at low level Temperature Inversion • A temperature inversion forms near the surface on a clear night with calm or light surface wind. • Wind just above the inversion may be relatively strong. • A wind shear zone develops between the calm and the stronger winds above.

Cont. • Eddies in the shear zone cause airspeed fluctuations as an aircraft climbs or descends through the inversion. • The fluctuation in airspeed can induce a stall when closer to the ground.

Cont. Wind shear in a zone between relatively calm wind below an inversion and strong wind above the inversion. This condition is most common at night or in early morning. It can cause an abrupt turbulence encounter at low altitude.

Cont. • How to fly the aircraft? • Takeoff may be in the direction of the wind above the inversion. If so, the aircraft encounters a sudden tailwind and a corresponding loss of airspeed when climbing through the inversion. Stall is possible. • If approach is into the wind above the inversion, the headwind is suddenly lost when descending through the inversion. Again, a sudden loss in airspeed may induce a stall.

Cont. • When taking off or landing in calm wind under clear skieswithin a few hours before or after sunrise, be prepared for a temperature inversion near the ground. • You can be relatively certain of a shear zone in the inversion if you know the wind at 2,000 to 4,000 feet is 25 knots or more. • Allow a margin of airspeed above normal climb or approach speed to avoid danger of stall in event of turbulence or sudden change in wind velocity.

Wind Shear in Frontal Zone • A front can be between two dry stable airmasses and can be empty of clouds. Even so, wind changes abruptly in the frontal zone and can induce wind shear turbulence. • The degree of turbulence depends on the magnitude of the wind shear. • To fly the aircraft: When turbulence is expected in a frontal zone, follow turbulence penetration procedures recommended in your aircraft manual. front : the atmospheric phenomenon created at the boundary between two different air masses

Wake Turbulence • An aircraft receives its lift by accelerating a mass of air downward. • Thus, whenever the wings are providing lift, air is forced downward under the wings generating rotary motions or vortices off the wing tips. • When the landing gear bears the entire weight of the aircraft, no wing tip vortices develop.

Cont. • These vortices continue throughout the flight and until the aircraft again settles firmly on its landing gear. Wake turbulence wing tip vortices developing as aircraft breaks ground. These vortices develop when the aircraft is rotated into a flying attitude and the wings begin developing lift.

Cont. • These vortices spread downward and outward from the flight path. They also drift with the wind. • Strength of the vortices is proportional to the weight of the aircraft as well as other factors. • Therefore, wake turbulence is more intense behind large, transport category aircraft than behind small aircraft. Generally, it is a problem only when following the larger aircraft.

Cont. • The turbulence persists several minutes and may remain present after the aircraft is out of sight.

How to fly the aircraft? • Most jets when taking off lift the nose wheel about midpoint in the takeoff roll; therefore, vortices begin about the middle of the takeoff roll. Vortices behind propeller aircraft begin only a short distance behind lift-off. • For a landing of either type of aircraft, vortices end at about the point where the nose wheel touches down. • Avoid flying through these vortices. More specifically, when using the same runway as a heavier aircraft.

Rule of takeoff and landing behind the Heavier Aircraft • If landing behind another aircraft, keep your approach above his approach and keep your touchdown beyond the point where his nose wheel touched the runway (figure A)

Cont. • if landing behind a departing aircraft, land only if you can complete your landing roll before reaching the midpointof his takeoff roll (figure B).

Cont. • if departing behind another departing aircraft, take off only if you can become airborne before reaching the midpoint of his takeoff roll and only if you can climb fast enough to stay above his flight path.

Cont. • if departing behind a landing aircraft, don't unless you can taxi onto the runway beyond the point at which his nose wheel touched down and have sufficient runway left for safe takeoff (figure D)

MET 2204 METEOROLOGY